RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 19, ES6006, doi:10.2205/2019ES000683, 2019

Figure 3. Non-dimensional average frequency, depending on the non-dimensional coordinate, calculated as $ < f > = \frac{1}{2\pi}$ $\frac{\int\omega n d\omega d\theta}{\int n d\omega d\theta}$, where $n(\omega,\theta)=\frac{\varepsilon(\omega,\theta)}{\omega}$ is the spectrum of the wave action, for wind velocity 10 m/sec (solid line). The dash-dotted line is the automodel dependence $3.4\cdot \left(\frac{xg}{U^{2}} \right)^{-0.3}$ with the fitting coefficient in front of it; dashed line - M1 approach; dash-dotted line – M2 approach.

 
Citation: Pushkarev Andrei (2019), On different approaches to statistical description of ocean waves, Russ. J. Earth Sci., 19, ES6006, doi:10.2205/2019ES000683.
 

Copyright 2019 by the Geophysical Center RAS.